54. If the temperature/dewpoint spread is small and decreasing, and the temperature is 62 degrees F, what type of weather is most likely to develop?
A. Freezing precipitation.
B. Thunderstorms.
C. Fog or low clouds.

55. In which situation is advection fog most likely to form?
A. A warm, moist air mass on the windward side of mountains.
B. An air mass moving inland from the coast in winter.
C. A light breeze blowing colder air out to sea.

56. What types of fog depend upon wind in order to exist?
A. Radiation fog and ice fog.
B. Steam fog and ground fog.
C. Advection fog and upslope fog.

57. Low-level turbulence can occur and icing can become hazardous in which type of fog?
A. Rain-induced fog.
B. Upslope fog.
C. Steam fog.

The weather that is most likely to develop with a small and decreasing temperature/dewpoint spread and a temperature of 62 Degrees F is fog or low clouds. Advection fog is most likely to form when a warm, moist air mass moves over a cold surface such as the windward side of mountains. Types of fog that depend on wind include advection fog and upslope fog. Low-level turbulence and hazardous icing can occur in rain-induced fog.

Explanation:

If the temperature/dewpoint spread is small and decreasing, and the temperature is 62 Degrees F, the most likely type of weather to develop is fog or low clouds. When the temperature and dewpoint are close together and decreasing, it indicates the saturation of the air and the formation of fog or low clouds. In this situation, the air has a high humidity level, resulting in the condensation of water vapor into visible cloud formations close to the ground.

Advection fog is most likely to form when a warm, moist air mass moves over a cold surface such as the windward side of mountains. The warm air cools rapidly as it encounters the colder surface, causing the water vapor to condense and fog to form. This type of fog is commonly observed along coastal areas, where warm, moist air moves over colder ocean waters.

The types of fog that depend upon wind in order to exist include advection fog and upslope fog. Advection fog forms when moist air moves horizontally over a colder surface, while upslope fog forms as moist air is forced up a slope or hillside. Both types require the movement of air and interaction with different temperature gradients to trigger the condensation of water vapor into fog.

In rain-induced fog, low-level turbulence can occur and icing can become hazardous. Rain-induced fog occurs when rain evaporates into the cool air near the surface, leading to the saturation of the air and the formation of fog. The presence of low-level turbulence and potential for icing make this type of fog dangerous for aviation and other activities.

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